Geologi Wilayah Desa Boidu, Kecamatan Bulango Utara, Kabupaten Bone Bolango

Regionally, intrusive rocks are quite widespread in the study area, belonging to the Diorite Bone (Tmb) formation. The formation is composed of Diorite, Quartz Diorite, Granodiorite and Adamellite. This study aims to determine the condition of lithology, geological structure and geomorphology. The method used in this research is expolrative, namely obtaining data directly from the field and then analyzing petrology and petrography laboratories. The geomorphology of the study area is divided into 2 geomorphological units, namely; intrusion hills and alluvial plain units. The study area is unofficially divided into three rock units when sorted from oldest to youngest, namely: Diorite rock unit, Granodiorite unit (Middle-Late Miocene), and alluvial sediment unit (Holocene). The geological structure of the study area consists of tensile bridging with a southwest - northeast direction.

Authors

Publication Details

Journal
Journal of Applied Geoscience and Engineering
Published
2025-06-30
DOI
https://doi.org/10.37905/jage.v4i1.30326
Primary Topic
Geological and Geophysical Studies
Type
article
Field-Weighted Citation Impact
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article

Geologi Wilayah Desa Boidu, Kecamatan Bulango Utara, Kabupaten Bone Bolango

Muhammad Kasim, Aang Panji Permana, Irka Priwanda Tumelap
Journal of Applied Geoscience and Engineering
Geological and Geophysical Studies
article

Geologi Wilayah Desa Boidu, Kecamatan Bulango Utara, Kabupaten Bone Bolango

Muhammad Kasim, Aang Panji Permana, Irka Priwanda Tumelap
article en

Abstract

Regionally, intrusive rocks are quite widespread in the study area, belonging to the Diorite Bone (Tmb) formation. The formation is composed of Diorite, Quartz Diorite, Granodiorite and Adamellite. This study aims to determine the condition of lithology, geological structure and geomorphology. The method used in this research is expolrative, namely obtaining data directly from the field and then analyzing petrology and petrography laboratories. The geomorphology of the study area is divided into 2 geomorphological units, namely; intrusion hills and alluvial plain units. The study area is unofficially divided into three rock units when sorted from oldest to youngest, namely: Diorite rock unit, Granodiorite unit (Middle-Late Miocene), and alluvial sediment unit (Holocene). The geological structure of the study area consists of tensile bridging with a southwest - northeast direction.

Journal of Applied Geoscience and EngineeringVol. 4(1)
Openalex Percentile: Top 66%
Geological and Geophysical Studies
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